Official Series Description


Lab Data Summary

Aggregate lab data for the KAHLER soil series. This aggregation is based on all pedons with a current taxon name of KAHLER, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to KAHLER were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
4771C0026S1971UT057001Kahler6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3194427,-111.8680573

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KAHLER soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the KAHLER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the KAHLER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the KAHLER series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with KAHLER share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the KAHLER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the KAHLER series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with KAHLER, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing KAHLER as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Kahler silt loam, bedrock substratum, 35 to 70 percent slopes12F13076103521hwor02119781:24000
McGarr-Kahler complex, 12 to 35 percent north slopes111D17766207222lbor60419881:24000
McGarr-Kahler complex, 35 to 60 percent north slopes111E16636207322lcor60419881:24000
Umatilla-Kahler-Gwin complex, 35 to 70 percent slopes5859CO32031202421nz0qor60720181:24000
Kahler ashy silt loam, 0 to 15 percent slopes6048AO731207581t1m7or60720181:24000
Kahler-Klickson-Tolo complex, 1 to 8 percent slopes4228AW7133852852ksvcor62620181:24000
Kahler stony ashy loam, 2 to 20 percent slopes4329AO423385413znj9or62620181:24000
Hutchley-Bocker-Kahler complex, 20 to 50 percent south slopes4323NO373385406znj4or62620181:24000
Tolo-Kahler-Silvies complex, 2 to 20 percent slopes4313AO2833853951vtl6or62620181:24000
Kahler-Linecreek-Getaway complex, 30 to 60 percent slopes5777CO49224373041r1p7or63120181:24000
Umatilla-Kahler-Gwin complex, 35 to 70 percent slopes5859CO33824868491nz0qor63120181:24000
Kahler-Linecreek-Getaway complex, 60 to 90 percent north slopes6065DN382437450nj72or63120181:24000
Kahler silt loam, bedrock substratum, 35 to 70 percent slopes92F2146140521wtor64819771:24000
Umatilla-Kahler-Gwin association, 35 to 70 percent slopes108F72290644202512or66719841:20000
Umatilla-Kahler association, 35 to 70 percent slopes107F9736644192511or66719841:20000
Kahler gravelly ashy loam, granite substratum, 35 to 70 percent slopes41F301664500253nor66719841:20000
Umatilla-Kahler association, 15 to 35 percent slopes107E1114644182510or66719841:20000
Kahler silt loam, 2 to 15 percent slopes40C70664498253lor66719841:20000
Kahler silt loam, 15 to 35 percent slopes40E34764499253mor66719841:20000
Kahler-Linecreek-Getaway complex, 30 to 60 percent north slopes1503130845232tykor67019991:24000
Kahler-Linecreek-Getaway complex, 60 to 90 percent north slopes1511097849982vfwor67019991:24000
Kahler-Anatone complex, 30 to 60 percent slopes148920845212tyhor67019991:24000
Kahler-Anatone-Rock outcrop complex, 60 to 90 percent slopes149132845222tyjor67019991:24000
Kahler gravelly loam, 6 to 10 percent slopesKaC770506569k03yut60919741:24000
Kahler gravelly loam, 3 to 6 percent slopesKaB330506568k03xut60919741:24000

Map of Series Extent

Approximate geographic distribution of the KAHLER soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .